رسالة جامعية

Investigating Seismic Wave Scattering in Heterogeneous Environments and Implications for Seismic Imaging

التفاصيل البيبلوغرافية
العنوان: Investigating Seismic Wave Scattering in Heterogeneous Environments and Implications for Seismic Imaging
المؤلفون: Bongajum, Emmanuel
المساهمون: Milkereit, Bernd
سنة النشر: 2011
المجموعة: Theses Canada / Thèses Canada (Library and Archives Canada)
مصطلحات موضوعية: seismic imaging, heterogeneity, scattering, stochastic modeling, geostatistics, transmission imaging, mineral exploration, wave propagation
الوصف: Inhomogeneities in the earth (fractures, layering, shape, composition) are responsible for seismic wave scattering and contribute towards amplitude, travel time, frequency and spectral fluctuations observed in seismic records. This thesis presents findings that complement our understanding of seismic scattering and imaging in heterogeneous media. Interest focused on probing the correlation between spatial variations in attributes that characterize the state (physical, chemical) of rocks and seismic waveform data with consideration towards potential implications for seismic survey design to optimize imaging, imaging with converted waves, microseismic monitoring, velocity modeling and imaging of lithological boundaries. The highlights of the research strategy include: • The use of stochastic methods to build realistic earth models that characterize the 1D, 2D and 3D spatial variations in rock properties. These petrophysical earth models are conditioned by experimental (“hard”) data such as geology, wave velocities and density from case study areas like the Bosumtwi impact crater and the base metal deposits in Nash Creek (Canada) and Thompson (Canada). The distributions of the sulfide mineralization at Nash Creek and at Thompson represent two end members of the heterogeneity spectrum. While the sulfide mineralization at Nash Creek is highly disseminated in nature, the sulfide rich zones at Thompson occur as well defined volumes (lens-shaped) having a strong density contrast with respect to the host rocks. • Analysis of modeled forward (transmitted) and backward scattered wave propagation in the heterogeneous earth models. As a result of a study aimed at correlating resonant frequencies to scale length parameters, it is observed that the efficiency of the spectral ratio method is undermined by its sensitivity to the interference between P- and S-waves as well as the impedance contrast. It is also demonstrated that travel time of direct arrivals (transmitted waves) can be used to infer structural heterogeneity and ...
نوع الوثيقة: thesis
اللغة: English
العلاقة: http://hdl.handle.net/1807/29667Test
الإتاحة: http://hdl.handle.net/1807/29667Test
رقم الانضمام: edsbas.AF84FD70
قاعدة البيانات: BASE